Open main menu
Home
Random
Recent changes
Special pages
Community portal
Preferences
About Wikipedia
Disclaimers
Incubator escapee wiki
Search
User menu
Talk
Dark mode
Contributions
Create account
Log in
Editing
Palmoxylon
(section)
Warning:
You are not logged in. Your IP address will be publicly visible if you make any edits. If you
log in
or
create an account
, your edits will be attributed to your username, along with other benefits.
Anti-spam check. Do
not
fill this in!
== Description == [[File:Palmoxylon sp. fossil - Botanischer Garten, Dresden, Germany - DSC08508.JPG|thumb|240px|left| Fossil specimen of ''Palmoxylon'']] Petrified palmwood includes a group of fossil woods that contain prominent rod-like structures within the regular grain of the silicified wood. Depending upon the angle at which they are cut by fracture, these rod-like structures show up as spots, tapering rods, or continuous lines. The rod-like structures are [[sclerenchyma]] bundles that comprise part of the woody tissues that gave the wood its vertical strength. Petrified palmwood is a favorite of [[Rockhounding|rock collectors]] because it is replaced by [[silica]] and exhibits well-defined rod-like structures and variety of colors. As a result, it exhibits a wide range of colors and designs when cut that can be incorporated into [[jewelry]] and other ornamental items. Because it is composed of silica, it is hard enough to polish and withstand the wear and tear of normal use.
Edit summary
(Briefly describe your changes)
By publishing changes, you agree to the
Terms of Use
, and you irrevocably agree to release your contribution under the
CC BY-SA 4.0 License
and the
GFDL
. You agree that a hyperlink or URL is sufficient attribution under the Creative Commons license.
Cancel
Editing help
(opens in new window)